
Fossil bivalve shell
Likely a fossilized oyster or other marine bivalve; exact genus is indeterminate from the image
AI-generated identification · may be incorrectCream to tan, flattened shell with radiating/concentric growth lines and possible mineral replacement. Original shell material is commonly calcite or aragonite; Mohs hardness about 3–4, dull to slightly silky luster, low cleavage, and specific gravity roughly 2.6–2.8.
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